Show simple item record

dc.contributor.authorYılmaz, Yücel
dc.date.accessioned2019-06-27T08:00:59Z
dc.date.available2019-06-27T08:00:59Z
dc.date.issued2003
dc.identifier.isbn3-540-43711-8
dc.identifier.urihttps://hdl.handle.net/20.500.12469/198
dc.identifier.urihttps://link.springer.com/chapter/10.1007%2F978-3-662-05308-9_5
dc.description.abstractThe Troia area and the surroundings in northwest Anatolia are located between two most active fault zones. These zones have developed under the influence of the north Anatolian fault system coupled with the Aegean N-S extension. These active fault systems have caused several severe earthquakes which damaged the Troia area. The morphology and geology of the region have evolved under strong tectonic control. Major morphological features of the region such as the gulfs of Saroz and Edremit the Canakkale (Dardanelles) Strait and the Kazdag high are young post-early Pliocene entities. They formed when the transtensional tectonic regime in the Aegean began. One of the major products of this system are the listric normal faults. They caused back-tilting of the down-thrown blocks which in turn diverted the major drainage to the north. As a result increasingly more clastic materials have been transported to the Troia area where a large alluvial plain has developed.
dc.language.isoEnglish
dc.publisherSpringer-Verlag Berlin
dc.titleSeismotectonics and geology of Troia and surrounding areas northwest Anatolia
dc.typeProceedings Paper
dc.identifier.startpage55
dc.identifier.endpage75
dc.relation.journalTroia and The Troad: Scientific Approaches
dc.identifier.wosWOS:000182073200005
dc.contributor.khasauthorYılmaz, Yücel


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record